E

There are many conventional theories that seek to explain the development
of a tornado. Without exception they cannot explain the complex internal
structure and energy flows in a simple and logical manner.

Tornados show a remarkably complex coherent structure, and the existence
of rope like tornados, tornadoes that kink and reform, and the nature of
the ejection zone at the tornado base all require, and can be simply explained
if air with or without particles can be shown to exist in a form that
has both shear and tensile strength.

The charged sheath vortex theory can explain the formation of the tornado
in a very simple and elegant way. It predicts the complex physical structure
and electrical properties of the tornado. It explains the simple basis
for many tornado ‘anomalies’ and also makes predictions about the structure
of the tornado that may not yet have been observed.

A vortex is produced by a spinning mass of air (or other gas or dust cloud),
but there are two different types of vortex in the air circulation that
we call a tornado with very distinct properties.

The Turbulence or Shear Vortex

The simplest is the turbulence vortex, or shear vortex. This is often seen
in a dust devil, where an air current flowing over a hot ground surface, rises.
As the air rises it starts to rotate, drawing air and dust in at ground level
and carrying it upwards through the rotating column to discharge at the top.
But note that a dust devil may rapidly become charged and turn into a charged
sheath vortex.

The shear vortex can also be seen at the tip of aircraft wings, particularly
in conditions of high relative humidity, where the vortex becomes visible
as moisture condenses in the lower pressure inside the vortex. These vortices
can persist for several minutes, and the large vortices produced by very
heavy aircraft can flip a light aircraft following behind. On rare occasions
a wingtip turbulence vortex will also become charged and turn into a charged
sheath vortex that will rip any following aircraft apart, however strongly
built they are.

Turbulence vortices are easy to produce by creating angled air currents
and an updraft. Demonstrations of 'tornados' are all turbulence vortices.
For one of the best see the experimental setup that created a turbulence
dust devil for a commercial at: http://www.reelefx.com/Tornado/40footVolvo.htm

Air can blow against an object and move and lift dust and light objects,
but has very little shear strength and so cannot transmit energy through
a column of air.

The shear vortex has ragged and turbulent edges, and the centre of the
vortex is also ragged in appearance.

The Charged Sheath Vortex

The charge sheath vortex develops within a large charge
cloud where the repulsion between the charges is cancelled out,1 ) Two stationary particles carrying the same electrical charge will
repel each other, but within an electric field they will form dipoles
that will experience an attractive force.
2 ) In a large charge cloud where the repulsion between the charges is the
same in all directions, this force will cancel out3 ) Two streams of dipoles with the same field charge moving
in parallel in a large charge cloud will also develop a force of attraction
through their electromagnetic interaction.

The charged sheath vortex is a fast spinning tube of
electrically charged air and/or dust molecules.

The high velocity of the particles, all with the same
net charge charge, and all rotating in the same direction, creates very
large electrodynamic forces (Very similar to an electrical solenoid that
produces a powerful electromagnet)

By a quirk of history, diagrams of electrical current
show the arrow for current direction for the movement of positive charge.
This makes no difference for the charge sheath, but can be a little confusing
for students of electricity at first.

The arrow on field lines is shown pointing to the south magnetic
pole. The direction shown by a compass.
The north pole on a magnetic compass points to a south magnetic
pole -(At the geographic north pole!)

This shows the magnetic field produced by a positive charge particle
moving. Note the way the thumb placed in the direction of movement and
the fingers showing the magnetic field.

If several charged particles move in parallel, the magnetic forces
between them draw them together.
We know from Z pinch experiments that the electromagnetic forces
that draw the particles togther is greater than the electrostatic charge
that pushes them apart.
When a moving charge passes through a magnetic field it experiences
a force which is perpendicular to both the magnetic field and the velocity.
- shown by the red dotted line in the following diagram. As the
particle responds to the force, by moving upwards, the force continues
to act perpendicular to the new path, and so the particle will be forced
into a circular path if it remains within the magnetic field..

But the moving charge particle also produces a magnetic field. Note
that the direction of the magnetic field produced by the charge particle
(arrows point to the south pole) is the opposite direction
in relation to the circular path of the charged particle as
in the diagram above. The charge particles are therefore cancelling the
magnetic field which caused the charge particle to follow a circular
path.

Consider the case where within a large charge cloud where
the repulsion between the charges is cancelled out a stream of positive
particles forms a loop in the absence of an externally applied magnetic
field. There is a powerful force of attraction between the particles moving
in parallel as in B above.
If a charged particle strays inwards into the inner field, the magnetic
force on the charged particle will subject the particle to a force
that pushes it back out into the sheath as discussed in C and D above.
If the charged particle strays outwards into a region where the field is
in the opposite direction, the force it is subject to will push it back
into the sheath.

1 ) Two stationary particles carrying the same electrical charge will
repel each other, but within an electric field they will form dipoles
that will experience an attractive force.
2 ) In a large charge cloud where the repulsion between the charges is the
same in all directions, this force will cancel out3 ) Two streams of dipoles with the same field charge moving
in parallel in a large charge cloud will also develop a force of attraction
through their electromagnetic interaction.

Within a large charge cloud where the repulsion between the charges is
cancelled out, the flow is held as a coherent stream by the attraction
between forces moving in parallel. Any instability in velocity will cause
greater magnetic fields in the faster region than the slower regions.
The faster region with the greater magnetic field will be pinched
more, speeding up the flow, which increases the pinch and so on
becoming longer and thinner. But the extension in length cannot be accommodated
in a straight line. It can only force the stream to form a loop.

Within a large charge cloud where the repulsion between the charges is
cancelled out, the vortex sheath is compressed between the powerful inward
and outward forces, accelerating and generating yet more powerful forces.
Since the outer force pushing inwards always remains the stronger, the vortex
will compress and narrow- until the forces generated by the opposing sheath
wall spinning in the opposite direction prevent further compression.
The force needed to turn the particles into the curve will
also increase as the velocity increases and radius of curvature increases
and will put a limit on the minimum radius the vortex can achieve.
Within the centre of the charged sheath vortex the fields
reinforce each other to produce a powerful solenoidal field.

These forces very powerfully keep the particles from
flying outwards away from the tube, but also prevent the tube collapsing
inwards. If new rotating charged material is constantly being added then
this will also push the ends of the tube away from the middle. The result
of this balance of very powerful forces is a tube that must stay almost
circular, with a clear central tube. Because all the particles are held
very firmly in place the sheath can transmit large amounts of energy from
one end to the other.

The charged sheath vortex is the mechanism capable of transmitting the
energy of a tornado from the clouds to the ground.

The centre of this tube may become visible as moisture condenses in the
lower pressure, and sometimes it will contain dust or water from the ground
surface.

Energy from the Storm

Occasionally in normal thunder clouds, and much more frequently in the
supercells in tornado alley, the airflow imparts a circular rotation to
a

large volume of thundercloud. This can arise as a single pronounced
curl to the storm, or shear between violently opposed air flow can create
a whole series of vortices all rotating in the same direction.

At the same time in the thunder clouds, charge becomes separated. The base
of the cloud is usually negatively charged and the tops positively charged.

An electrical field strength of 10000 N/C is typical for this charge cloud.
The charged, rotating cloud mass may have a volume of several cubic kilometers.
It has a huge kinetic energy resulting from its rotation, and it is this
kinetic energy that is transferred to the tornado.

1 ) Two stationary particles carrying the same electrical charge will
repel each other, but within an electric field they will form dipoles
that will experience an attractive force.
2 ) In a large charge cloud where the repulsion between the charges is the
same in all directions, this force will cancel out3 ) Two streams of dipoles with the same field charge moving
in parallel in a large charge cloud will also develop a force of attraction
through their electromagnetic interaction. If the charge is
sufficiently entrained in the air, the dipole particles cannot simply be
pushed through the air mass.
If the net charge on the dipoles is sufficiently high, then the repulsion
will try and cause the air mass to expand. This expansion will be opposed
by the air pressure of the surrounding air. This would result in the storm
cloud having a slightly lower density than the surrounding air. If the net
charge on the dipoles is slightly lower, the least energy configuration is
where the positive charge on one dipole lines up with the negative charge
on the nearest dipoles. This produces a force of attraction between the dipoles.
We can represent this equilibrium as: static field=(expanded charge repulsion
field)=(charge repulsion of field)+(air pressure)
Now consider that the cloud is rotating. As we have agreed before, this
will produce a slight force of attraction between the paths of the moving
dipoles through interaction of their magnetic fields.

The moving charges will move (slightly) closer together until the (attraction
through magnetic field)+(static field)=(static field)+(charge repulsion
through closer proximity).

However slight, our stream of charged particles is now moving faster, and
through conservation of angular momentum, will cause the storm to rotate
with a narrower radius.

Our faster stream of particles now produces a (slightly) larger magnetic
field, so again it will accelerate and charge carriers will move closer
together, increasing the field strength until magnetic field=charge repulsion.

However as the rotation of the storm increases, a new factor comes into
play. The faster air flow of the rotation stream results in a lower effective
air pressure.
This permits further movement of the charge carriers into the faster flowing
region, and a higher field strength
The new equilibrium is now:
magnetic field=charge repulsion+ external air pressure - internal pressure of rotating
air.

Each iteration of the equation results in a faster, thinner vortex tube.

Collisions between particles and the electromagnetic force generated by
the overall mass of moving dipoles will cause some charge particles to be
transferred - with a net flow inward. The magnetic fields will thus result
in the development of an electric field, with the highest charge in the central
region of the vortex tube. This electric field ensures that the dipoles in
the rotating airstream remain orientated as dipoles, with the opposite charge
to the central core facing inwards.

As the charged particles in the cloud rotate, the electrodynamic forces
their movement creates draw them together and inwards. Because the energy
must stay constant, particles moving in a smaller circle must move faster
- in order to conserve angular momentum they must speed up. Think
of the ice skater spinning, speeding up as she draws in her arms to her
body.
The forces of attraction between the particles must increase as they
speed up and the forces between the charged particles increase dramatically
as the distances get smaller.
This makes the electrodynamic forces stronger still, so the process
of moving inwards and spinning faster continues until a charged sheath vortex
is being produced at the centre of the rotating storm.

The sheath is a shell of dipole particles entraining the air. It displays
a gradient of charge from the highest charge in the centre to the lowest
charge on its outer surface. It is a combination of the hydrodynamic pressures,
electromagnetic fields and electric fields on the dipoles and air.

If the circulation is disrupted by a kink, the region away from the driving
force of the storm cloud flys apart - demonstarting that this is not simply
a falling vortex of air.
The forces created by an electrical current in a wire are produced in proportion
to the speed of electrons through a wire. Because of collisions and random
movements of electrons in the wire, the overall speed of the electrons, or
drift speed is quite slow. (but the density is high). A 1 volt potential
in a pure copper wire will produce a drift speed of 0.0043m/s This is less
than half a centimetre in a second.
By contrast air flow in a tornado can exceed 1000 m/s. This is not
the true speed of the electrons, which are still moving very much faster,
but repeated colliding within the dipole particle.
The forces between moving electrons in a mass flow may be thousands
of times greater than the forces between electrons in a wire.

If these electrodynamic forces were not present the maximum voltage
gradient in air is about 3*10^6 volts / m before an electrical discharge
takes place. Measurements of higher charge gradients in the sheath of dust
devils demonstrates very clearly the charge sheath at work.

Pressure from new charged dipole particles joining the sheath now forces
the ends of the tube outwards, up into the cloud, and down towards the opposite
charge on the ground.

In a small tornado only the charged vortex sheath approaches the ground,
and this may not be visible until dust starts to outline it. A large tornado
may show a large inverted cone as the pressure of the electrodynamic forces
creates downward pressure on the cloud base well outside the charged vortex
sheath. This maintains the charge cloud external to the charge sheath,
so that the electrostatic repulsion does not come to predominate.

As the charge sheath is pushed down below the charge cloud of the thunderstorm
it will start to attract an external sheath of charged particles with the
opposite charge. This external sheath is not rotating and so does not cancel
the electromagnetic fields produced by the charge sheath, but does balance
the electrostatic charge. Charge is continually being pushed down this charge
sheath and being neutralised by external charge, but because of the excellent
insulating properties of air, this neutralisation process is slow relative
to the movement of charge within the tornado.

Occasionaly a tornado tube is seen to fly apart. This would suggests a
point where neutralisation of the sheath has taken place, or where electrostatic
repulsion is now greater than electromagnetic attraction.

Touch down

Large dust and debris clouds often obscure the processes
at work at the ground.

The charged vortex sheath bites into the ground rather like a hole cutter.
A tubular narrow blade rotating at high speed moving over the ground surface.
The external charge cloud which maintains the balance of forces between
the sheath and the external medium is not shown on these diagrams.

Because it has a high electrical charge, it induces the opposite charge
onto everything near it. The attractive forces are huge and together with
the abrasion of particles rotating in the sheath it rips the surface from
anything it touches. As these ripped off particles start to speed up the
electrodynamic force come into play and the particles that were violently
attracted are now violently ejected.

See the movie from http://redrock.ncsa.uiuc.edu/~jewett/Obs/May1598.html
This is Overview
This is a good sequence starting with charged sheath vortex touching
down, clearly visible as a thin tube. An ejection cloud starts to build
up and an outer turbulence vortex starts to form, but is then blown away
- ahead of the vortex - by the surface wind. The outer turbulence vortex
then reforms, and by the time it crosses the road is extremely well defined.
At around 16 seconds part of the turbulence vortex is again breaking up
in a large curl, again blown out by a wind moving faster than the vortex
is travelling

Ejection Zone

If you watch a small tornado closely you can see these
forces at work. Watch how the opposite charged dust from the ground is
thrown out at high speed and then seems to drift downward again. This shows
very clearly that at this stage there is almost no airflow coming down the
tornado or going up the tornado. See the movie from http://www.uni-stuttgart.de/Wetter/specials/movies/tornado2.mpg
Look at the time between 00.03 to 00.06 A small tubular charged sheath
vortex is visible inside the larger turbulence vortex.

Charge Particle Expansion creates a Turbulence Vortex

As the ejected charged dust cloud increases, the charge
between the dust and the charged air molecules create a pressure that forces
the particles apart and reduces the density. This charge induced reduction
in density makes the ejection cloud lighter than the surrounding air so
it starts to rise.

As this dust cloud rises it draws air in from round the base of the tornado,
and this rising air may also start to rotate, but at a much slower rate
than the charged sheath vortex spinning at high speed inside it.

The result is a turbulence vortex of dust and air rising, surrounding
the charged sheath vortex of the tornado at its centre.

The Anatomy of a Large Tornado

When we watch a large tornado, what we see is the rising
turbulence vortex of dust and debris, but at its core it is powered by
a charged sheath vortex of extreme ferocity and strength. From http://www.kwtv.com/wx/wxcenter.htm
is tornado2.mov(389K)
A or tornado2.mov from cache A
huge tornado, but most of what we can see are hanging plumes of ejected
material, in a gently rising and gently rotating air stream. The violence
of the charged sheath at the core is not visible.

When we examine the debris field after the tornado has passed, the broadest
part is a band of destruction caused by the inflowing winds of the turbulence
vortex, but at the core is a narrow band that has felt the teeth of the
charged sheath itself and the ground surface shows the striations as the
surface was pulled apart. Small debris such as straw can become entrained
in the charged sheath and then behaves as though it was part of a rigid solid,
driving the debris through wood or steel. The charged sheath can also rip
and twist metal structures under the ground surface protected from any wind,
but fully exposed to the violent magnetic fields at the end of the vortex
tube.

All the points made can be demonstrated by clips from video of real storms.
Many of these are available on the Internet.

From http://www.kwtv.com/wx/wxcenter.htm
is tornado1.mov(857K)
Or from cacheThis is particularly
interesting. Not only can we see the charged sheath vortex within the
turbulence vortex, but the charged vortex sheath appears to kink and then
violently fly apart at 05 to 06. The kink demonstrates that there is no
major vertical airflow within the charged sheath vortex.

From http://redrock.ncsa.uiuc.edu/~jewett/Obs/May1598.html
is Overview
Or from cache This is a
good sequence starting with charged sheath vortex touching down, clearly
visible as a thin tube. An ejection cloud starts to build up and an outer
turbulence vortex starts to form, but is then blown away - ahead of the
vortex - by the surface wind. The outer turbulence vortex then reforms,
and by the time it crosses the road is extremely well defined. At around
16 seconds part of the turbulence vortex is again breaking up in a large
curl, again blown out by a wind moving faster than the vortex is travelling

http://www.iphc.org/drusa/tornado/vidclip5.html
One of a sequence of the same storm as the rotating storm clip. Notice
the outer turbulence vortex is not showing much vertical movement, and
no inflow visible at ground level, but notice large debris being ejected
up and out and then falling down from the right.

At the top of the tornado the vortex tube is pushed up above the storm.
Here there is no debris to mark its rotation, but any charged particle
within the vortex tube that is not rotating in the sheath will be violently
repelled by the electrostatic charge of the sheath and ejected out through
the ends of the vortex tube. These high energy particles will ionise the
thin air in fountains above the tornado tube. These have been photographed
from space and are known as sprites.

There is another natural phenomenon, described in numerous reports with
a wealth of incidental detail, yet whose structure and development is still
unexplained: Ball lightning

You are welcome to join the discussion, but
please note that any claims you make for or against these theories should
be backed by scientific reasoning that can be developed from first principles.

This information is copyright Peter Thomson 2001-2004

tornado fusion Charge sheath vortex basics for tornado

ggggghhggfttfyyf

ok i have one question what does shear mean

How useful is this message about tornado fusion Charge sheath vortex basics for tornado?